Global Warming Images
 
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IMG_8708.jpg A school field trip on the cliff tops at Durdle Door on the Dorset coast near Lulworth, UK, with a flock of Rooks flying past.
 
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IMG_0824.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8754.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8756.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8762.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8768.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8776.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8790.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8795.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8797.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8801.jpg A Nodding Donkey oil pump at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8802.jpg Wytch farm oil well at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8807.jpg Wytch farm oil well at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8812.jpg Wytch farm oil well at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_8815.jpg Wytch farm oil well at Kimmeridge Bay, Dorset, the only onshore oil reserves in the UK .
 
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IMG_0145.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0154.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0160.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0168.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0171.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0174.jpg A fisherman landing whelks destined for the Asian market on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0189.jpg A fisherman landing whelks destined for the Asian market, as well as crabs and lobster on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0197.jpg A fisherman landing whelks destined for the Asian market, as well as crabs and lobster on the Cob at Lyme Regis, part of the World Heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0082.jpg A tree toppled by a severe storm in a wooded section of the undercliff, between Seaton and Lyme Regis on the World heritage site of the Jurassic Coast, Dorset, UK.
 
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IMG_0086.jpg A women negotiates a tree toppled by a severe storm in a wooded section of the undercliff, between Seaton and Lyme Regis on the World heritage site of the Jurassic Coast, Dorset, UK.
 
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File0364.jpg Solar panels on an old house on the Dorset coast near Charmouth, UK.
 
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20120609_IMG_9667.jpg A bus in Lyme Regis , Dorset, part of the World heritage Site of the Jurassic Coast. UK.
 
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20120609_IMG_9700.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9705.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9713.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9719.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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File0340.jpg A street name in Charmouth, Dorset, UK, seems rather prescient in predicting climate change induced sea level rise.
 
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File0344.jpg A Wood Pigeon (Columba palumbus) sits on a signpost pointing to Lower Sea Lane in Charmouth, Dorset, UK, lower seas being highly unlikely due to climate change induced sea leve rise,
 
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File0347.jpg A street name in Charmouth, Dorset, UK, seems rather prescient in predicting climate change induced sea level rise.
 
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IMG_0034.jpg A storm surge steel gate closed following a bad storm in Seaton, to protect the town against flooding, Dorset, UK.
 
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IMG_0036.jpg A storm surge steel gate closed following a bad storm in Seaton, to protect the town against flooding, Dorset, UK.
 
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IMG_0037.jpg A storm surge steel gate closed following a bad storm in Seaton, to protect the town against flooding, Dorset, UK.
 
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IMG_0042.jpg A storm surge steel gate closed following a bad storm in Seaton, to protect the town against flooding, Dorset, UK.
 
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IMG_0135.jpg The Cob at Lyme Regis, on the World Heritage site of the Jurassic Coast, Dorset, UK. It has recently been extended to provie protection to the town from increasing storm surges and climate change induced sea level rise.
 
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IMG_0137.jpg The Cob at Lyme Regis, on the World Heritage site of the Jurassic Coast, Dorset, UK. It has recently been extended to provie protection to the town from increasing storm surges and climate change induced sea level rise.
 
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20120609_IMG_9694.jpg A sign about a diversion due to landslips on the South West Coast Path between Lyme Regis and Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9698.jpg A sign about a diversion due to landslips on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9702.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9709.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9717.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9720.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9727.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9728.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9734.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9740.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9746.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9755.jpg A tear in the ground showing where the next landslip will take place on the South West Coast Path near Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9756.jpg A landslip on the South West Coast Path at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9757.jpg A tear in the ground showing where the next landslip will take place on the South West Coast Path near Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9758.jpg A tear in the ground showing where the next landslip will take place on the South West Coast Path near Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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20120609_IMG_9759.jpg A tear in the ground showing where the next landslip will take place on the South West Coast Path near Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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File0333.jpg A sign about a diversion due to landslips on the South West Coast Path between Lyme Regis and Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heav rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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File0349.jpg A massive landslip at Black Ven between Lyme Regis and Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heavy rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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File0354.jpg A massive landslip at Black Ven between Lyme Regis and Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heavy rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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File0357.jpg A section of coastal cliff on the Jurassic Coast between Charmouth and bridport that is slumping into the sea.
 
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File0362.jpg A section of coastal cliff on the Jurassic Coast between Charmouth and bridport that is slumping into the sea.
 
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IMG_0659.jpg A massive landslip at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heavy rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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IMG_0673.jpg A wellingotn boot trapped in the mud of a massive landslip at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heavy rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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IMG_0684.jpg A landslip at Charmouth. This section of the Jurassic Coast has always been prone to landslips due to the unstable nature of the Jurassic clays and shales, but increased heavy rainfall events and rising sea levels driven by climate change are starting to lead to an increased incidence of coastal erosion.
 
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